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i Detection of Smoke and Dust Aerosols Using Multi-sensor Satellite ...

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with cloud in some areas along the CALIPSO path. In the Fig. 5.6, the BTD (12, 11μm) is<br />

positive at three peaks with latitude 36.59 0 N - 39.79 0 N, 41.04 0 N - 44.02 0 N, <strong>and</strong> 44.640<br />

N - 45.750 N, which is corresponding to dust aerosol areas. Between three peaks, the<br />

BTD (12, 11μm) is negative which corresponding to cloud. Therefore, four dust aerosol<br />

layers are found <strong>and</strong> marked with black circle in Fig. 5.7.<br />

After the successful detection, the detail information about dust aerosol could be<br />

further retrieved. Fig. 5.8 shows the total attenuated backscatter signal pr<strong>of</strong>ile at 532 nm<br />

in two locations: (40 0 N, 109.16 0 E) <strong>and</strong> (42 0 N, 108.51 0 E). The vertical pr<strong>of</strong>ile for specific<br />

location gives more detail <strong>and</strong> accurate values about dust aerosols. At the first location,<br />

cloud (in dashed line rectangular) floated about 10.5 km above the sea level. At the<br />

latitude 42 0 N, a large backscatter value at the altitude 2.5 km is corresponding to the dust<br />

storm. By integrating the measurements <strong>of</strong> both <strong>sensor</strong>s, the vertical <strong>and</strong> horizontal<br />

information about dust aerosol can be retrieved. Table 5.3 summarized the vertical <strong>and</strong><br />

horizontal information about dust aerosols occurred in 2008 spring season in northwest<br />

China, including height, averaged depth, width, <strong>and</strong> coverage.<br />

71

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